The Earth's atmosphere – A stable isotope perspective and review

This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isoto...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Hoefs, Jochen [verfasserIn] Harmon, Russell [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Übergeordnetes Werk:	Enthalten in: Applied geochemistry - Amsterdam [u.a.] : Elsevier Science, 1986, 143
Übergeordnetes Werk:	volume:143

DOI / URN:	10.1016/j.apgeochem.2022.105355

Katalog-ID:	ELV010115277

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allfields	10.1016/j.apgeochem.2022.105355 doi (DE-627)ELV010115277 (ELSEVIER)S0883-2927(22)00159-7 DE-627 ger DE-627 rda eng 550 VZ 38.32 bkl Hoefs, Jochen verfasserin aut The Earth's atmosphere – A stable isotope perspective and review 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future. Harmon, Russell verfasserin (orcid)0000-0003-1967-3611 aut Enthalten in Applied geochemistry Amsterdam [u.a.] : Elsevier Science, 1986 143 Online-Ressource (DE-627)306648091 (DE-600)1499242-5 (DE-576)08198426X nnns volume:143 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie VZ AR 143
spelling	10.1016/j.apgeochem.2022.105355 doi (DE-627)ELV010115277 (ELSEVIER)S0883-2927(22)00159-7 DE-627 ger DE-627 rda eng 550 VZ 38.32 bkl Hoefs, Jochen verfasserin aut The Earth's atmosphere – A stable isotope perspective and review 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future. Harmon, Russell verfasserin (orcid)0000-0003-1967-3611 aut Enthalten in Applied geochemistry Amsterdam [u.a.] : Elsevier Science, 1986 143 Online-Ressource (DE-627)306648091 (DE-600)1499242-5 (DE-576)08198426X nnns volume:143 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie VZ AR 143
allfields_unstemmed	10.1016/j.apgeochem.2022.105355 doi (DE-627)ELV010115277 (ELSEVIER)S0883-2927(22)00159-7 DE-627 ger DE-627 rda eng 550 VZ 38.32 bkl Hoefs, Jochen verfasserin aut The Earth's atmosphere – A stable isotope perspective and review 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future. Harmon, Russell verfasserin (orcid)0000-0003-1967-3611 aut Enthalten in Applied geochemistry Amsterdam [u.a.] : Elsevier Science, 1986 143 Online-Ressource (DE-627)306648091 (DE-600)1499242-5 (DE-576)08198426X nnns volume:143 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie VZ AR 143
allfieldsGer	10.1016/j.apgeochem.2022.105355 doi (DE-627)ELV010115277 (ELSEVIER)S0883-2927(22)00159-7 DE-627 ger DE-627 rda eng 550 VZ 38.32 bkl Hoefs, Jochen verfasserin aut The Earth's atmosphere – A stable isotope perspective and review 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future. Harmon, Russell verfasserin (orcid)0000-0003-1967-3611 aut Enthalten in Applied geochemistry Amsterdam [u.a.] : Elsevier Science, 1986 143 Online-Ressource (DE-627)306648091 (DE-600)1499242-5 (DE-576)08198426X nnns volume:143 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie VZ AR 143
allfieldsSound	10.1016/j.apgeochem.2022.105355 doi (DE-627)ELV010115277 (ELSEVIER)S0883-2927(22)00159-7 DE-627 ger DE-627 rda eng 550 VZ 38.32 bkl Hoefs, Jochen verfasserin aut The Earth's atmosphere – A stable isotope perspective and review 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future. Harmon, Russell verfasserin (orcid)0000-0003-1967-3611 aut Enthalten in Applied geochemistry Amsterdam [u.a.] : Elsevier Science, 1986 143 Online-Ressource (DE-627)306648091 (DE-600)1499242-5 (DE-576)08198426X nnns volume:143 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie VZ AR 143
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title	The Earth's atmosphere – A stable isotope perspective and review
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title_full	The Earth's atmosphere – A stable isotope perspective and review
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title_sort	the earth's atmosphere – a stable isotope perspective and review
title_auth	The Earth's atmosphere – A stable isotope perspective and review
abstract	This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future.
abstractGer	This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future.
abstract_unstemmed	This review summarizes the stable isotope composition of the gases and aerosols comprising the Earth's atmosphere. Recent technical progress in analytical methodologies has enabled analysis the H- and O-isotopic composition of water vapor by remote sensing, precise measurement of the rare isotopes 17O, 33S and 36S, the recognition of mass-independent isotope fractionations, and determination of the stable isotope composition of volatile metals in aerosols. Together these approaches have resulted in new insights into atmospheric processes and permitted the delineation of atmospheric constituents derived from natural versus anthropogenic sources. Ice core analysis has demonstrated that the isotope composition of the atmosphere has changed continuously as a consequence of both past climate cycles and more recently because of fossil fuel and other anthropogenic emissions. Isotope proxies and geochemical modeling have recognized that the nature of the atmosphere has varied throughout geologic history and will continue to do so in the near future.
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title_short	The Earth's atmosphere – A stable isotope perspective and review
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up_date	2024-07-06T16:52:28.372Z
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The Earth's atmosphere – A stable isotope perspective and review

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